Sxey ertera vedo
The Nabro volcano is a caldera that has seen explosive eruptions in the past, so this new intrusion could have interacted with pre-existing mush under the volcano or this new basaltic intrusion might have just had a lot of water dissolved in the magma.
Further investigation of the initial ash will likely solve this problem.
However, with limited staff and resources, we simply cannot respond to all who write to us.
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You can see the black-and-red advancing basaltic lava flow (looks like a`a) that is the very end of the lava flow.
In terms of temperature, basaltic lava is much hotter than rhyolite or even andesite lava, so it should appear to be quite hot in any thermal image of the volcano (but how hot exactly is trickier and requires some guesses about the composition before we know the composition).
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